Abstract
Crack propagation can gradually reduce the strength of the rock and eventually result in rock failure. Coupling effect of stress and seepage in fracture could accelerate the rock failure process. In this work, a set of water sealing device is developed to apply different fluid pressures in the pre-existing fracture in specimens made of rock-like material. We have carried out uniaxial compression tests on specimens at different pre-existing flaw dip angles (30°, 45°, and 60°) coupled with fluid pressures in the fracture. Through laboratory experiments and numerical simulations, we find that without fluid pressure in the pre-existing flaw, wing cracks and secondary cracks appear at the pre-existing flaw tips. With the increase of the fluid pressure in the flaw, the propagation of secondary cracks is restrained, no secondary cracks appear at the flaw tips. The increase of fluid pressure accelerates the wing crack propagation, inhibits the secondary cracks, and causes the specimen to undergo tensile failure. Compared with the specimen without the fluid pressure in the flaw, the fluid pressure in the flaw promotes wing crack initiation and propagation, and causes the initiation stress of the wing cracks and the peak strength of the specimens to decrease gradually. With or without fluid pressure in the fracture with the increase of the flaw dip angle, the initiation stress of wing cracks and peak strength of the specimen first decrease and then increase. When the pre-existing flaw dip angle is 45°, the peak strength and the initiation stress are the lowest.
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Abbreviations
- \(a\) :
-
Half-length of the pre-existing flaw
- \(C\) :
-
Cohesion
- \(f_{i}\) :
-
Body force
- \(g_{x}\),\(g_{x}\),\(g_{x}\) :
-
Acceleration of gravity in the x, y, and z directions
- \(K\) :
-
Stiffness matrix
- \(M\) :
-
Mass matrix
- \(C\) :
-
Damping matrix
- \(K_{\rm I}\),\(K_{{{\rm I}{\rm I}}}\) :
-
Mode I and II stress intensity factor, respectively
- \(P\) :
-
Total nodal pressure
- \(p_{p}\) :
-
Seepage pressure
- \(Q(t)\) :
-
Loading vector
- \(u_{i}\) :
-
Nodal displacement
- \(\dot{u}_{i}\) :
-
Nodal velocity
- \(\alpha\) :
-
Angle between the minimum principal stress direction and the pre-existing flaw
- \(\rho\) :
-
Density
- \(s\) :
-
Nodal saturation
- \(\tau\) :
-
Shear strength
- \(\tau_{f}\) :
-
Shear stress on the crack surface
- \(\phi\) :
-
Internal friction angle
- \(\gamma\) :
-
Specific gravity
- \(\sigma_{1}\),\(\sigma_{3}\) :
-
Maximum and minimum principal stresses, respectively
- \(\sigma_{N}\),\(\sigma_{T}\) :
-
Normal and transverse compressive stresses, respectively
- \(\overline{\sigma }_{t}\) :
-
Tensile strength
- \(\sigma_{ij.j}\) :
-
The first-order partial derivative of the stress tensor
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Acknowledgements
This work is funded by the National Natural Science Foundation of China (Nos. 51879151, 41672281, 51909142), and the Fundamental Research Funds of Shandong University (No. 2017JC001). These resources of support are gratefully acknowledged.
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Wei, C., Zhang, B., Zhu, W. et al. Fracture Propagation of Rock like Material with a Fluid-Infiltrated Pre-existing Flaw Under Uniaxial Compression. Rock Mech Rock Eng 54, 875–891 (2021). https://doi.org/10.1007/s00603-020-02256-3
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DOI: https://doi.org/10.1007/s00603-020-02256-3